Semilir eruption
| Semilir eruption | |
|---|---|
| Date | 21 million years ago |
| Type | Ultra-Plinian |
| Location | East Java, Indonesia |
The Semilir eruption was a major volcanic event which took place in Indonesia during the Early
Geology Background
Java is between
Eruption Product
The volcanic deposits are fresh and dip uniformly towards the south at approximately 30°. The sequence is divided into three formations which are, from base to top, the Kebobutak, Semilir and Nglanggran Formations (note that Kebobutak Formation is not a same eruption event with Semilir and Nglanggran). The top part of Kebobutak Formation are intensely
Facies of Semilir Formation
In East Java the base of the Semilir Formation can be identified by the abrupt termination of bioturbated reworked deposits characteristic of the Kebobutak Formation. The volcanic rocks of the Semilir Formation are characterised by features typical of terrestrial air-fall, pyroclastic surge and flow deposits including dune and antidune structures, crystal layering, well-sorted granular laminations, diffuse bedding, breccias (with metre-scale pumice blocks), thick mantling ashes, and abundant fragments of charcoal. Locally there are water-laid deposits, with scoured irregular bases, flame, traction and suspension structures, and large slump folds indicating an unstable marine slope. Smyth et al. (2011) interpret these observations to indicate the Semilir Formation was erupted in a subaerial setting in which pyroclastic flows travelled across vegetated slopes picking up and baking plant fragments, with some of these flows entering the sea. Some of the primary material would have been redeposited as lahars in distal settings.[1]
Facies of Nglanggran Formation
Overlying the Semilir Formation is a 200 to 500 m (660 to 1,640 ft) thick sequence of massive, resistant, monomict andesitic volcanic breccias, crystal-rich sandstones and minor lava flows of the Nglanggran Formation. The breccia beds are 1 to 10 m (3.3 to 32.8 ft) thick and can be mapped for several kilometres. Interbedded crystal-rich sand- stones are much thinner. The breccias are both clast- and matrix-supported with angular fragments commonly 2 to 75 cm (0.79 to 29.53 in) across with some blocks up to 3 m (9.8 ft). Fragment imbrication within the breccias records diverging west and southwest flow from a source in the northeast part of the Batu Agung Escarpment. There is no evidence of any marine influence, and we interpret the Nglanggran Formation as terrestrial deposits formed by sector or repeated dome collapse, marking the end of arc activity in the Southern Mountains. The top and base of the Nglanggran Formation forms topographic breaks in slope, because the andesitic breccias are much more resistant than the underlying and overlying units, and the feature and the formation can be easily mapped across the area over a distance of 46 km (29 mi).[1]
Thickness and distribution
Based on examined exposures, measured sections and published geological maps, the combined thickness of the Semilir and Nglanggran Formations is between 250 and 1,200 m (820 and 3,940 ft), exposed over 800 km2 (310 sq mi), and the total volume of volcanic material at least 500 km3 (120 cu mi) (DRE). Widely distributed volcanic quartz-rich sandstones of Early Miocene age exposed in East Java that may be Semilir products but have not been precisely dated. One such sandstone is the Jaten Formation, exposed near Pacitan, 80 km (50 mi) east of the Batu Agung Escarpment. The location and character of this formation are described in detail in Smyth et al. (2008).[2] Zircons from the Jaten Formation have a weighted mean SIMS age of 19.6 ± 0.5 Ma and this is consistent with them being reworked products of the Semilir eruption.[1]
References
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